scholarly journals The Role of Lithospheric Flexure in the Landscape Evolution of the Wilkes Subglacial Basin and Transantarctic Mountains, East Antarctica

2019 ◽  
Vol 124 (3) ◽  
pp. 812-829 ◽  
Author(s):  
Guy J. G. Paxman ◽  
Stewart S. R. Jamieson ◽  
Fausto Ferraccioli ◽  
Michael J. Bentley ◽  
Neil Ross ◽  
...  
2005 ◽  
Vol 45 (1-3) ◽  
pp. 35-49 ◽  
Author(s):  
S.S.R. Jamieson ◽  
N.R.J. Hulton ◽  
D.E. Sugden ◽  
A.J. Payne ◽  
J. Taylor

Water ◽  
2021 ◽  
Vol 13 (11) ◽  
pp. 1608
Author(s):  
Salvatore Ivo Giano

This Special Issue deals with the role of fluvial geomorphology in landscape evolution and the impact of human activities on fluvial systems, which require river restoration and management [...]


2014 ◽  
Vol 41 (17) ◽  
pp. 6199-6206 ◽  
Author(s):  
Irina V. Gorodetskaya ◽  
Maria Tsukernik ◽  
Kim Claes ◽  
Martin F. Ralph ◽  
William D. Neff ◽  
...  

2021 ◽  
Vol 59 (4) ◽  
pp. 357-376
Author(s):  
N. M. Sushchevskaya ◽  
A. V. Sobolev ◽  
G. L. Leitchenkov ◽  
V. G. Batanova ◽  
B. V. Belyatsky ◽  
...  
Keyword(s):  

2011 ◽  
Vol 236 (1-2) ◽  
pp. 34-47 ◽  
Author(s):  
John F. Shroder ◽  
Lewis A. Owen ◽  
Yeong Bae Seong ◽  
Michael P. Bishop ◽  
Andrew Bush ◽  
...  

Author(s):  
Milad Hooshyar ◽  
Shashank Anand ◽  
Amilcare Porporato

Landscapes evolve towards surfaces with complex networks of channels and ridges in response to climatic and tectonic forcing. Here, we analyse variational principles giving rise to minimalist models of landscape evolution as a system of partial differential equations that capture the essential dynamics of sediment and water balances. Our results show that in the absence of diffusive soil transport the steady-state surface extremizes the average domain elevation. Depending on the exponent m of the specific drainage area in the erosion term, the critical surfaces are either minima (0 <  m  < 1) or maxima ( m  > 1), with m  = 1 corresponding to a saddle point. We establish a connection between landscape evolution models and optimal channel networks and elucidate the role of diffusion in the governing variational principles.


2020 ◽  
Vol 6 (3) ◽  
pp. 349-383 ◽  
Author(s):  
Thomas M. Claybourn ◽  
Christian B. Skovsted ◽  
Lars E. Holmer ◽  
Bing Pan ◽  
Paul M. Myrow ◽  
...  

2004 ◽  
Vol 78 (6) ◽  
pp. 1146-1153 ◽  
Author(s):  
Derek W. Kellogg ◽  
Edith L. Taylor

Despite their importance in breaking down lignified tissue today, much is still unknown about the role of mites in the fossil record, especially with reference to the Paleozoic–Mesozoic transition. This study examines permineralized peat from three localities in the central Transantarctic Mountains, ranging in age from Permian to Jurassic, for evidence of diversity and abundance of wood-boring mites. Evidence of mites, in the form of coprolites and tunnels in wood and other tissues, was found at all three localities; the Triassic site included more than 10 times as many wood borings as the Permian site. Our results supplement prior evidence of wood-boring mites during the Mesozoic and thereby fill in the known geologic range of this plant/animal interaction.


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